When crocodiles roamed the Arctic

WHEN Ernest Shackleton and his men marched towards the South Pole in December 1908, they came across something entirely unexpected. After scaling the vast Beardmore glacier on the edge of the polar plateau, they found seams of coal amid the snow and ice. They also found impressions of leaves in sandstone boulders nearby and even fossilised wood from a coniferous tree.

The conclusion was extraordinary but inescapable: Antarctica was once warm and forested, conditions that could hardly be more different to the far-below-freezing midsummer weather that forced Shackleton's team to turn back before reaching the pole. How was this possible?

Four years later, Alfred Wegener put forward his theory of continental drift which, it was later realised, could explain the balmy climate: Antarctica had been warmer because it was once much closer to the equator. Even today, some schoolchildren are taught that continental drift accounts for all the evidence for ...

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